際際滷shows by User: DemitrisAnastasiou / http://www.slideshare.net/images/logo.gif 際際滷shows by User: DemitrisAnastasiou / Tue, 09 Mar 2021 15:16:07 GMT 際際滷Share feed for 際際滷shows by User: DemitrisAnastasiou DSO Thessaly report_09032021 /slideshow/dso-thessaly-report09032021/244080483 dsothessalyreport09032021-210309151608
Preliminary analysis results for continuous GNSS stations at Thessaly (3 & 4/03/2021)]]>
Preliminary analysis results for continuous GNSS stations at Thessaly (3 & 4/03/2021)]]> Tue, 09 Mar 2021 15:16:07 GMT /slideshow/dso-thessaly-report09032021/244080483 DemitrisAnastasiou@slideshare.net(DemitrisAnastasiou) DSO Thessaly report_09032021 DemitrisAnastasiou Preliminary analysis results for continuous GNSS stations at Thessaly (3 & 4/03/2021) <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/dsothessalyreport09032021-210309151608-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Preliminary analysis results for continuous GNSS stations at Thessaly (3 &amp; 4/03/2021)
DSO Thessaly report_09032021 from Demitris Anastasiou
]]> 87 0 https://cdn.slidesharecdn.com/ss_thumbnails/dsothessalyreport09032021-210309151608-thumbnail.jpg?width=120&height=120&fit=bounds document Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Geodetic and seismological analysis of the January 26th, 2014 Cephalonia Island earthquake sequence /slideshow/geodetic-and-seismological-analysis-of-the-january-26th-2014-cephalonia-island-earthquake-sequence/57729681 iugg15cephalonia-160201120554
On January 26, 2014 a strong earthquake of magnitude Mw=5.8 occurred on Cephalonia Island followed by a similar magnitude earthquake Mw=5.7 one week later on February 3, 2014. Extensive structural damages, landslides and many damages on the islands' main roads, harbour and airport caused mainly on the western and central part of the island. The first event located 2km eastern of Lixouri town and was followed five hours later by a strong aftershock of magnitude Mw=5.3. The second strong earthquake located in the north part of Paliki eninsula North-East Cephalonia). Geodetic data of six permanent GNSS stations were available and analysed in this study both in pro and post seismic terms, using 30sec and 1Hz data where available. The time series analysis shows the effect of each event at nearby stations. Seismological data are used to determine the focal mechanisms of the earthquake sequence and an attempt to investigate the homogeneity of the mechanisms and the stress field of the area is presented in the study. Geodetic analysis and seismological results are used to understand the mechanism of the events.]]>
On January 26, 2014 a strong earthquake of magnitude Mw=5.8 occurred on Cephalonia Island followed by a similar magnitude earthquake Mw=5.7 one week later on February 3, 2014. Extensive structural damages, landslides and many damages on the islands' main roads, harbour and airport caused mainly on the western and central part of the island. The first event located 2km eastern of Lixouri town and was followed five hours later by a strong aftershock of magnitude Mw=5.3. The second strong earthquake located in the north part of Paliki eninsula North-East Cephalonia). Geodetic data of six permanent GNSS stations were available and analysed in this study both in pro and post seismic terms, using 30sec and 1Hz data where available. The time series analysis shows the effect of each event at nearby stations. Seismological data are used to determine the focal mechanisms of the earthquake sequence and an attempt to investigate the homogeneity of the mechanisms and the stress field of the area is presented in the study. Geodetic analysis and seismological results are used to understand the mechanism of the events.]]> Mon, 01 Feb 2016 12:05:54 GMT /slideshow/geodetic-and-seismological-analysis-of-the-january-26th-2014-cephalonia-island-earthquake-sequence/57729681 DemitrisAnastasiou@slideshare.net(DemitrisAnastasiou) Geodetic and seismological analysis of the January 26th, 2014 Cephalonia Island earthquake sequence DemitrisAnastasiou On January 26, 2014 a strong earthquake of magnitude Mw=5.8 occurred on Cephalonia Island followed by a similar magnitude earthquake Mw=5.7 one week later on February 3, 2014. Extensive structural damages, landslides and many damages on the islands' main roads, harbour and airport caused mainly on the western and central part of the island. The first event located 2km eastern of Lixouri town and was followed five hours later by a strong aftershock of magnitude Mw=5.3. The second strong earthquake located in the north part of Paliki eninsula North-East Cephalonia). Geodetic data of six permanent GNSS stations were available and analysed in this study both in pro and post seismic terms, using 30sec and 1Hz data where available. The time series analysis shows the effect of each event at nearby stations. Seismological data are used to determine the focal mechanisms of the earthquake sequence and an attempt to investigate the homogeneity of the mechanisms and the stress field of the area is presented in the study. Geodetic analysis and seismological results are used to understand the mechanism of the events. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/iugg15cephalonia-160201120554-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> On January 26, 2014 a strong earthquake of magnitude Mw=5.8 occurred on Cephalonia Island followed by a similar magnitude earthquake Mw=5.7 one week later on February 3, 2014. Extensive structural damages, landslides and many damages on the islands&#39; main roads, harbour and airport caused mainly on the western and central part of the island. The first event located 2km eastern of Lixouri town and was followed five hours later by a strong aftershock of magnitude Mw=5.3. The second strong earthquake located in the north part of Paliki eninsula North-East Cephalonia). Geodetic data of six permanent GNSS stations were available and analysed in this study both in pro and post seismic terms, using 30sec and 1Hz data where available. The time series analysis shows the effect of each event at nearby stations. Seismological data are used to determine the focal mechanisms of the earthquake sequence and an attempt to investigate the homogeneity of the mechanisms and the stress field of the area is presented in the study. Geodetic analysis and seismological results are used to understand the mechanism of the events.
Geodetic and seismological analysis of the January 26th, 2014 Cephalonia Island earthquake sequence from Demitris Anastasiou
]]> 226 5 https://cdn.slidesharecdn.com/ss_thumbnails/iugg15cephalonia-160201120554-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 https://public.slidesharecdn.com/v2/images/profile-picture.png https://cdn.slidesharecdn.com/ss_thumbnails/dsothessalyreport09032021-210309151608-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/dso-thessaly-report09032021/244080483 DSO Thessaly report_09... https://cdn.slidesharecdn.com/ss_thumbnails/iugg15cephalonia-160201120554-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/geodetic-and-seismological-analysis-of-the-january-26th-2014-cephalonia-island-earthquake-sequence/57729681 Geodetic and seismolog...